Atmosphere-ocean InteractionClarendon Press, 1972 - 275 pages |
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Page 209
... hurricane crosses a coastline . With hurricane winds it is not possible to neglect the squares and products of the horizontal velocity components even in the boundary layer . For steady axially - symmetric storms , the integrated ...
... hurricane crosses a coastline . With hurricane winds it is not possible to neglect the squares and products of the horizontal velocity components even in the boundary layer . For steady axially - symmetric storms , the integrated ...
Page 210
... hurricane area . His findings suggest that a tropical cyclone consumes more water vapour and latent heat than can be obtained from the pre - existing undisturbed tropical atmosphere . The hurricane must collect vapour from the ocean to ...
... hurricane area . His findings suggest that a tropical cyclone consumes more water vapour and latent heat than can be obtained from the pre - existing undisturbed tropical atmosphere . The hurricane must collect vapour from the ocean to ...
Page 265
... hurricane : Part I. J. atmos . Sci . 24 ( 2 ) , 197-207 . OOYAMA , K. ( 1969 ) Numerical simulation of the life cycle of tropical cyclones . J. atmos . Sci . 26 ( 1 ) , 3–40 . OSTLUND , H. G. ( 1967 ) Hurricane tritium I : preliminary ...
... hurricane : Part I. J. atmos . Sci . 24 ( 2 ) , 197-207 . OOYAMA , K. ( 1969 ) Numerical simulation of the life cycle of tropical cyclones . J. atmos . Sci . 26 ( 1 ) , 3–40 . OSTLUND , H. G. ( 1967 ) Hurricane tritium I : preliminary ...
Contents
INTRODUCTION | 1 |
THE STATE OF MATTER NEAR THE INTERFACE | 41 |
RADIATION | 71 |
Copyright | |
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advection air-sea amplitude angle approximately atmosphere average baroclinic barotropic bubbles cause changes circulation cloud components constant convection convergence Coriolis force decrease denotes diffusion direction dissipation drag coefficient eddy effect Ekman layer equation equilibrium expression flow fluctuations fluid flux Fourier frequency friction function geostrophic gravity waves group velocity height horizontal hurricane increase inertial integral interaction interface kinetic energy larger latitude linear mean mixed layer moisture molecular momentum motion observations ocean parameter perturbations phase velocity planetary boundary layer potential temperature processes propagation radiance ratio region relatively represents resulting Reynolds number Reynolds stress Rossby waves salinity scale sea surface sea water sensible heat shear specific humidity specified spectral spectrum storm term thermocline transport tropical turbulent unstable upwelling vapour pressure variable variations vector vertical viscosity vorticity wave number wavelength wind stress wind velocity yields zero дх